Articles | Volume 15, issue 5
https://doi.org/10.5194/gmd-15-2013-2022
https://doi.org/10.5194/gmd-15-2013-2022
Model description paper
 | 
10 Mar 2022
Model description paper |  | 10 Mar 2022

Global simulation of dissolved 231Pa and 230Th in the ocean and the sedimentary 231Pa∕230Th ratios with the ocean general circulation model COCO ver4.0

Yusuke Sasaki, Hidetaka Kobayashi, and Akira Oka

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on Sasaki et al.', Anonymous Referee #1, 24 Jun 2021
    • AC1: 'Reply on RC1', Akira Oka, 03 Sep 2021
  • RC2: 'Comment on gmd-2021-5', Anonymous Referee #2, 26 Jul 2021
    • AC2: 'Reply on RC2', Akira Oka, 03 Sep 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Akira Oka on behalf of the Authors (08 Oct 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (25 Oct 2021) by Paul Halloran
RR by Anonymous Referee #2 (15 Nov 2021)
RR by Anonymous Referee #1 (22 Nov 2021)
ED: Reconsider after major revisions (06 Dec 2021) by Paul Halloran
AR by Akira Oka on behalf of the Authors (26 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (03 Feb 2022) by Paul Halloran
AR by Akira Oka on behalf of the Authors (10 Feb 2022)  Author's response    Manuscript
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Short summary
For realistically simulating the recently observed distributions of dissolved 230Th and 231Pa in the ocean, we highlight the importance of the removal process of 231Pa and 230Th at the seafloor (bottom scavenging) and the dependence of scavenging efficiency on particle concentration. We show that consideration of these two processes can well reproduce not only the oceanic distribution of 231Pa and 230Th but also the sedimentary 231Pa/230Th ratios.